The pressingtogether of layers ofsnow under theirown weight. Overtime, it helpstransform snow intodense glacier ice.The buildup ofsnow over timewhen moresnow falls thanmelts.A series of linkedchanges in whichan initial changeleads to furtherchanges thatamplify the originaleffect.A gas in theatmosphere that ispart of the carboncycle. Increasing itcan contribute towarming byincreasing the energyEarth retains.The layer of gasessurrounding Earth. Itcontains carbondioxide and othergases that affect howenergy movesthrough the climatesystem.An increase in theaverage height of theocean surface. It canresult from warmingocean water expandingand from melting landice adding water to theocean.The pathEarth followsaround theSun.The process bywhich gases in theatmosphere absorband re-emit some ofthe energy leavingEarth, helping theplanet retain heat.Deviation from whatis expected ornormal. It can be adata point,observation, or resultthat doesn't fit theestablished pattern,model, or baseline.A climate feedback inwhich melting snowand ice expose darkersurfaces. Thosesurfaces reflect lesssunlight and absorbmore energy, whichcan cause additionalwarming and melting.All of Earth’swater, includingoceans, lakes,rivers,groundwater, andwater in theatmosphere.A long periodwhen Earth’sclimate is colderand glaciers andice sheets coverlarger areas thanthey do today.Changes over timein the Sun’senergy output. Itcan influenceEarth’s climate,especially oversome time scales.Ice thatforms whenocean waterfreezes.A piece of landice, usuallyfrom a glacier,that breaks offand enters theocean.A series of linkedchanges in whichthe effects counteror limit an initialchange, helpingstabilize a system.Water with very littledissolved salt.Glaciers store it onland, and seasonalglacial melt cansupply water topeople andecosystems.A weak acid thatforms when carbondioxide dissolves inwater, includingrainwater. It cancontribute to thechemical weatheringof rocks.The movement ofcarbon amongEarth’s systems,including theatmosphere,oceans, soil, rocks,and living things.The solid partsof Earth,includingrocks, soil, andsediments.The angle of Earth’srotational axisrelative to its orbit.Changes in this tilthappen over longperiods and canaffect the distributionof sunlight on Earth.The breaking down ofrocks and other Earthmaterials over time.Rainwater containingcarbonic acid cancontribute tochemical weathering.The long-termpattern oftemperature andother weatherconditions in aplace or acrossEarth.The release ofmaterial such aslava, gases, and ashfrom a volcano. It canaffect climate,including by addingparticles and gasesto the atmosphere.A large mass ofice formed onland when snowaccumulates andcompacts overmany years.The amountof incomingsunlight asurfacereflects.The pressingtogether of layers ofsnow under theirown weight. Overtime, it helpstransform snow intodense glacier ice.The buildup ofsnow over timewhen moresnow falls thanmelts.A series of linkedchanges in whichan initial changeleads to furtherchanges thatamplify the originaleffect.A gas in theatmosphere that ispart of the carboncycle. Increasing itcan contribute towarming byincreasing the energyEarth retains.The layer of gasessurrounding Earth. Itcontains carbondioxide and othergases that affect howenergy movesthrough the climatesystem.An increase in theaverage height of theocean surface. It canresult from warmingocean water expandingand from melting landice adding water to theocean.The pathEarth followsaround theSun.The process bywhich gases in theatmosphere absorband re-emit some ofthe energy leavingEarth, helping theplanet retain heat.Deviation from whatis expected ornormal. It can be adata point,observation, or resultthat doesn't fit theestablished pattern,model, or baseline.A climate feedback inwhich melting snowand ice expose darkersurfaces. Thosesurfaces reflect lesssunlight and absorbmore energy, whichcan cause additionalwarming and melting.All of Earth’swater, includingoceans, lakes,rivers,groundwater, andwater in theatmosphere.A long periodwhen Earth’sclimate is colderand glaciers andice sheets coverlarger areas thanthey do today.Changes over timein the Sun’senergy output. Itcan influenceEarth’s climate,especially oversome time scales.Ice thatforms whenocean waterfreezes.A piece of landice, usuallyfrom a glacier,that breaks offand enters theocean.A series of linkedchanges in whichthe effects counteror limit an initialchange, helpingstabilize a system.Water with very littledissolved salt.Glaciers store it onland, and seasonalglacial melt cansupply water topeople andecosystems.A weak acid thatforms when carbondioxide dissolves inwater, includingrainwater. It cancontribute to thechemical weatheringof rocks.The movement ofcarbon amongEarth’s systems,including theatmosphere,oceans, soil, rocks,and living things.The solid partsof Earth,includingrocks, soil, andsediments.The angle of Earth’srotational axisrelative to its orbit.Changes in this tilthappen over longperiods and canaffect the distributionof sunlight on Earth.The breaking down ofrocks and other Earthmaterials over time.Rainwater containingcarbonic acid cancontribute tochemical weathering.The long-termpattern oftemperature andother weatherconditions in aplace or acrossEarth.The release ofmaterial such aslava, gases, and ashfrom a volcano. It canaffect climate,including by addingparticles and gasesto the atmosphere.A large mass ofice formed onland when snowaccumulates andcompacts overmany years.The amountof incomingsunlight asurfacereflects.

Untitled Bingo - Call List

(Print) Use this randomly generated list as your call list when playing the game. There is no need to say the BINGO column name. Place some kind of mark (like an X, a checkmark, a dot, tally mark, etc) on each cell as you announce it, to keep track. You can also cut out each item, place them in a bag and pull words from the bag.


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  1. The pressing together of layers of snow under their own weight. Over time, it helps transform snow into dense glacier ice.
  2. The buildup of snow over time when more snow falls than melts.
  3. A series of linked changes in which an initial change leads to further changes that amplify the original effect.
  4. A gas in the atmosphere that is part of the carbon cycle. Increasing it can contribute to warming by increasing the energy Earth retains.
  5. The layer of gases surrounding Earth. It contains carbon dioxide and other gases that affect how energy moves through the climate system.
  6. An increase in the average height of the ocean surface. It can result from warming ocean water expanding and from melting land ice adding water to the ocean.
  7. The path Earth follows around the Sun.
  8. The process by which gases in the atmosphere absorb and re-emit some of the energy leaving Earth, helping the planet retain heat.
  9. Deviation from what is expected or normal. It can be a data point, observation, or result that doesn't fit the established pattern, model, or baseline.
  10. A climate feedback in which melting snow and ice expose darker surfaces. Those surfaces reflect less sunlight and absorb more energy, which can cause additional warming and melting.
  11. All of Earth’s water, including oceans, lakes, rivers, groundwater, and water in the atmosphere.
  12. A long period when Earth’s climate is colder and glaciers and ice sheets cover larger areas than they do today.
  13. Changes over time in the Sun’s energy output. It can influence Earth’s climate, especially over some time scales.
  14. Ice that forms when ocean water freezes.
  15. A piece of land ice, usually from a glacier, that breaks off and enters the ocean.
  16. A series of linked changes in which the effects counter or limit an initial change, helping stabilize a system.
  17. Water with very little dissolved salt. Glaciers store it on land, and seasonal glacial melt can supply water to people and ecosystems.
  18. A weak acid that forms when carbon dioxide dissolves in water, including rainwater. It can contribute to the chemical weathering of rocks.
  19. The movement of carbon among Earth’s systems, including the atmosphere, oceans, soil, rocks, and living things.
  20. The solid parts of Earth, including rocks, soil, and sediments.
  21. The angle of Earth’s rotational axis relative to its orbit. Changes in this tilt happen over long periods and can affect the distribution of sunlight on Earth.
  22. The breaking down of rocks and other Earth materials over time. Rainwater containing carbonic acid can contribute to chemical weathering.
  23. The long-term pattern of temperature and other weather conditions in a place or across Earth.
  24. The release of material such as lava, gases, and ash from a volcano. It can affect climate, including by adding particles and gases to the atmosphere.
  25. A large mass of ice formed on land when snow accumulates and compacts over many years.
  26. The amount of incoming sunlight a surface reflects.